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- W4236088492 abstract "The original crust of the McCartys flow, near McCartys in Valencia County, New Mexico, is, in restricted areas, broken up into blocks which are turned up on end and capsized like cakes of ice in an ice jam. Many of these blocks are deeply grooved and scratched. These grooves were formed when the bottoms of these blocks, still soft and plastic, were thrust across the irregular solid edges of other blocks. Pressure ridges are common on the McCartys flow. The medial cracks of many pressure ridges contain triangular wedges of lava whose thin edges point upward. The most striking feature about these wedges is their vertically grooved and fluted surfaces. The triangular wedges were formed when plastic lava was pushed up through a progressively widening medial crack. The irregularities of the wall rock at the bottom of the medial cracks, past which the plastic lava was pushed, produced the grooves and flutes." @default.
- W4236088492 created "2022-05-12" @default.
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- W4236088492 date "1938-05-01" @default.
- W4236088492 modified "2023-10-03" @default.
- W4236088492 title "Grooved Lava" @default.
- W4236088492 doi "https://doi.org/10.1086/624661" @default.
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